Researchers at Leeds University in northern England said two computer models highlighted the impact of so-called "very short-lived substances" -- VSLS -- that deplete the stratospheric shield.
The damage they do to the ozone layer is significant and likely to increase, they said, as emissions of man-made chlorine gases rise.
Ironically, one of the chemicals named in the report, dichloromethane, is used in the manufacture of substitutes for ozone-depleting gases outlawed by the UN's 1987 Montreal Protocol.
They are not covered by the landmark Montreal Protocol that requires the phaseout of longer-lasting chlorofluorocarbon (CFCs) and halon gases.
"Our model simulations indicate that VSLS account for a significant portion of ozone loss in the stratosphere," lead investigator Ryan Hossaini told AFP by email.
"In the Antarctic region, where the ozone hole forms each year and where ozone decreases are the most dramatic, we estimate that VSLS account for about 12.5 per cent of the total ozone loss.
"Globally averaged, the ozone loss due to VSLS in the lower stratosphere could be as much as 25 per cent, though it is much smaller at higher altitude."
The rest is man-made chlorine gases, and their contribution to the VSLS total is rising fast.
"Dichloromethane appears to be one of the most abundant man-made VSLS that we know of," said Hossaini.
Compared with the notorious CFCs, dichloromethane's impact today is small. The computer models suggest it reduces the ozone layer by less than one percent, he said.
"However, our study also shows that the atmospheric concentration of dichloromethane has increased dramatically in recent years," said Hossaini.
"At some locations its atmospheric concentration has doubled since the late 1990s."
Ozone is a three-atom molecule of oxygen. At ground level, as a byproduct of traffic pollution, it can be a dangerous respiratory irritant.
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